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<br />~ - '-j <br /> <br /> <br /> <br />............,.. <br /> <br />r.~.":! <br />;.1 <br /> <br />I; <br /><# <br />, <br />/ <br /> <br />..., <br /> <br />N <br /> <br />W*E <br /> <br />s <br /> <br />t ~ <br />'''.-of <br /> <br />Craig <br />6., <br />\ <br />140 <br /> <br />P1 <br />r..::, <br />[J <br /> <br />JrAA_ 1 <br />"'l7p DUFF <br />Af~~ <br />~~ <br /> <br />F1 <br />:1 <br />LJ <br /> <br />00;' <br />Figure 1. Location of the two study sites on the Yampa River, the Sevens at River Mile 63 <br />and Duffy at River Mile 109.5. <br /> <br />f I <br /> <br />have not been consistently above the median (which is 128 cfs) for the last five years (Figure <br /> <br />d <br /> <br /> <br />~.-.....-.....'...... <br />c",: <br /> <br />'<.-' <br /> <br />3). The minimum flow in 1999 was 168 cfs and 115 cfs in 1998. The 10-day minimum flow <br /> <br />for both 1998 (179 cfs) and 1999 (212 cfs) however has been above the median (153 cfs) <br /> <br />indicating that base flow conditions during the last two years have also been medial <br /> <br />fi <br />L.. <br />IJ <br /> <br />(Figure 3). <br /> <br />I 1 <br />: J <br />i ;.-; <br />f i <br />i ; <br /> <br />Gage records for Maybell (RM86) were compared to gage records from above the <br /> <br />Maybell diversion canal (RM 89) by combining flow from the Yampa River at Craig (RM <br /> <br />134) and the Williams Fork at its confluence with the Yampa (RM 130). Gage recording <br /> <br />f, l <br />~ ~ <br />'i .~ <br />bd <br /> <br />began for Craig and William Fork in October 1984, so the comparison represents the last 15 <br /> <br />r-1 <br />; . ~ <br />r"-J <br />k) <br /> <br />5 <br />